Post-glacial Foraminifera of the incised Yangtze paleo-valley and paleoenvironmental implications

doi:10.1017/jpa.2017.66

CORC > 南京地质古生物研究所 > 中国科学院南京地质古生物研究所 > 中国科学院南京地质古生物研究所

	Post-glacial Foraminifera of the incised Yangtze paleo-valley and paleoenvironmental implications
	Xue Ke; Baohua Li (李保华); Zongyan Zhang; Yi Wei; Fei Hu; Dongwen Fan; Li Sun; Jianlei Xie; Junjie Yu; Huazhou Yao
刊名	Journal of Paleontology
	2017
卷号	91 期号:6 页码:1102-1122
ISSN号	0022-3360
DOI	10.1017/jpa.2017.66
英文摘要	Three gravity cores (LZK1, ZKA4, and CSJA6) from the incised Yangtze paleo-valley comprise a thick sequence of the post-glacial deposit. Nineteen genera (26 species) of the benthic foraminifers are described from these cores, with detailed down-core foraminiferal variations to investigate their paleoenvironmental implications. Three foraminiferal assemblages are recognized for the lower, middle, and upper parts of the cores respectively. The lower part is dominated by Ammonia beccarii var. and Florilus decorus with lower abundance and diversity. In the middle part, the foraminifers are abundant and diverse, dominated by both Ammonia beccarii var. and Elphidium advenum. Cavarotalia annectens, Pararotalia nipponica, and porcellaneous benthic foraminiferal forms are always present, sometimes abundant. The upper part is characterized by the Ammonia beccarii-Elphidium magellanicum assemblage, except for the Core ZKA4, which is barren of foraminifers in this interval. AMS C-14 dates and foraminiferal assemblages both confirm that the transgression-regression sequence in these cores belongs to the "Ammonia transgression" during the Holocene. In addition to documenting the post-glacial sea-level fluctuations, the benthic foraminifers also reflect a warmer climate during the early-middle Holocene. The foraminiferal differences among the three cores can be used to interpret the influence of seawater during the post-glacial sea-level fluctuations. The area in the vicinity of Core ZKA4 was affected by marine water only during the middle Holocene, which was much shorter than the areas of the other cores.
WOS研究方向	Paleontology
语种	英语
出版者	CAMBRIDGE UNIV PRESS
WOS记录号	WOS:000413662100002
内容类型	期刊论文
源URL	[http://ir.nigpas.ac.cn/handle/332004/14040]
专题	中国科学院南京地质古生物研究所南京地质古生物研究所_其他
通讯作者	Baohua Li (李保华)
推荐引用方式 GB/T 7714	Xue Ke,Baohua Li ,Zongyan Zhang,et al. Post-glacial Foraminifera of the incised Yangtze paleo-valley and paleoenvironmental implications[J]. Journal of Paleontology,2017,91(6):1102-1122.
APA	Xue Ke.,Baohua Li .,Zongyan Zhang.,Yi Wei.,Fei Hu.,...&Huazhou Yao.(2017).Post-glacial Foraminifera of the incised Yangtze paleo-valley and paleoenvironmental implications.Journal of Paleontology,91(6),1102-1122.
MLA	Xue Ke,et al."Post-glacial Foraminifera of the incised Yangtze paleo-valley and paleoenvironmental implications".Journal of Paleontology 91.6(2017):1102-1122.